Ecological significance of nitrogen cycling by tubificid communities in shallow eutrophic lakes of the Danube Delta

摘要

Importance of tubificid populations on nitrogen cycle in two categories of shallow eutrophic lakes in the Danube Delta was quantitatively assessed for the 1992-1993 period.The structure of the primary producers in the studied lakes was used to discriminate between the two categories: (i) lakes dominated by macro-phytes (Ai) and (ii) lakes dominated by phytoplankton (A2).In both categories tubificid worms represented important fraction of the entire benthic community (35 and 32%,respectively,as number of individuals).They influence the sediment-water exchange of nutrients.The main processes involved are excretion of nutrients and their continuous release from sediments by molecular diffusion or through channels created by bioturbation.Inorganic nitrogen released from bottom sediments may regulate nitrogen load in the water body and thus,phytoplankton production.In 1992-1993,nitrogen stocks in tubificid biomass accounted for 5.3% in A,lakes and 15.6% in A2 lakes of the amount stocked in phytoplankton,and only for 1.2 and 2.9% respectively,of the nitrogen load in water body.Nitrogen excretion rates ranged between 60.52 and 153.74 mg N nT2 year"1,and release rates from sediments between 378.26 and 960.87 mg N m~2 year"1,the lowest values being recorded for A2 category.Differences are related to tubificid biomass,structure and abundance of primary producers and to nutrient load in different ecosystems.Ratios between release rate of inorganic nitrogen by tubificid worms and sedimentation rate of organic nitrogen in the two categories of lakes were 8.3 and 6.4% respectively.Contribution of nitrogen released daily from sediments to the dissolved inorganic nitrogen load in the water column was less than 0.5%.However,in A! and A2 lakes,the released nitrogen had a potential to sustain 24.74 and 8.01%,respectively,of the annual phytoplankton production.These values suggest the significance of tubificids in keeping the eutrophication process at a high level,especially during the periods when nitrogen is the main limiting factor for phytoplankton production.